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Soils and Regolith
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Pedology- The study of soils
Pedogenic processes depend on: ClORPTH Climate - Temperature, H2O, freezing Organisms - Addition and digestion of Org. Material Relief - Slope Steepness - Balance with erosion Parent Material - what do you start with? Time - How long has it been sitting there? Humans - Addition of fertilizer, tillage, salinization, etc… FLUX SITE
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The importance of soils
Life on Earth depends on soil Soil is a vital non-renewable resource It takes > 1000’s of years to form a soil Chemical weathering happens in soils
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Soil Degradation (erosion)
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The Dust Bowl
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Soil Horizons E/A2
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Soil Formation
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Clay Formation in Soils
Primary 2:1 1:1 0:1
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Some Soil Profiles Oxisol Alfisol Aridisol
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Soil Water
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Climate and Organisms
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Relief
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Parent Material
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Time
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Naming Soils Soils are named on the basis of Subsurface horizons
Layers in the soil that reflect soil forming processes
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Soil Orders Alfisols - Moderate temperature forests
Andisols - Soils on volcanic material Aridisols - Soils from deserts Entisols - Little soil formation Gelisols - Soils in cold regions w/ permafrost Histisols - Soils on peat Inceptisols - Young soils Mollisols - Grassland soils Oxisols - Tropical forests Spodosols - Cool, wet coniferous forests Ultisols - Tropical and subtropical forests Vertisols - Soils with cracks
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Global Soil Distribution
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Major Terrestrial Biomes
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